Interannual Variations of Indian Summer Monsoon in a GCM: External Conditions versus Internal Feedbacks
Open Access
- 1 April 1998
- journal article
- research article
- Published by American Meteorological Society in Journal of Climate
- Vol. 11 (4) , 501-522
- https://doi.org/10.1175/1520-0442(1998)011<0501:ivoism>2.0.co;2
Abstract
The potential predictability of the Indian summer monsoon due to slowly varying sea surface temperature (SST) forcing is examined. Factors responsible for limiting the predictability are also investigated. Three multiyear simulations with the R30 version of the Geophysical Fluid Dynamics Laboratory’s climate model are carried out for this purpose. The mean monsoon simulated by this model is realistic including the mean summer precipitation over the Indian continent. The interannual variability of the large-scale component of the monsoon such as the “monsoon shear index” and its teleconnection with Pacific SST is well simulated by the model in a 15-yr integration with observed SST as boundary condition. On regional scales, the skill in simulating the interannual variability of precipitation over the Indian continent by the model is rather modest and its simultaneous correlation with eastern Pacific SST is negative but poor as observed. The poor predictability of precipitation over the Indian regio... Abstract The potential predictability of the Indian summer monsoon due to slowly varying sea surface temperature (SST) forcing is examined. Factors responsible for limiting the predictability are also investigated. Three multiyear simulations with the R30 version of the Geophysical Fluid Dynamics Laboratory’s climate model are carried out for this purpose. The mean monsoon simulated by this model is realistic including the mean summer precipitation over the Indian continent. The interannual variability of the large-scale component of the monsoon such as the “monsoon shear index” and its teleconnection with Pacific SST is well simulated by the model in a 15-yr integration with observed SST as boundary condition. On regional scales, the skill in simulating the interannual variability of precipitation over the Indian continent by the model is rather modest and its simultaneous correlation with eastern Pacific SST is negative but poor as observed. The poor predictability of precipitation over the Indian regio...This publication has 2 references indexed in Scilit:
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- The Relationship Between Eastern Equatorial Pacific Sea Surface Temperatures and Rainfall over India and Sri LankaMonthly Weather Review, 1983